18

Jul

2016

How is climate change affecting Polar Regions? Part 2 – Professor Roger Barry

Written by: Roger Barry

 
Professor Roger Barry discusses climate change in polar regions
 

What is the most exciting research going on at each of the Poles currently?

In the Arctic there are major efforts to understand the drivers of the irregular decline in sea ice extent and thickness since the 1980s-90s.
Multiple sensors (satellite and buoys) provide high-resolution data spanning 35 years and sparse historical records, from whaling ships especially, are being used to build a record back to 1850 to characterize previous conditions.
Statistical and physical models are being applied to the seasonal prediction of the annual September ice minimum to understand its high inter-annual variability.

In Antarctica, recent work is exploring the susceptibility of the West Antarctic ice sheet to a ‘rapid’ decrease in mass through incursion of warm ocean water beneath the major fringing ice shelves. Projections indicate a potential rise of global sea level of 2 m by 2100 and 6 m by 2500 as a result of Antarctic ice loss..

How is climate change affecting Polar Regions? Are there different effects at each Pole?

The Arctic is experiencing global warming rates at two to three times above the global average. This “polar amplification” is due mainly to ice-albedo feedbacks; ice and snow melt exposes dark ocean and bare land that absorbs increased amounts of solar radiation that further raise temperatures thereby melting more ice and so on.  Arctic sea ice has been rapidly shrinking and thinning since the 1980s-90s. Permafrost is thawing near the surface, leading to ground subsidence and lake formation. Arctic glaciers and ice caps are losing mass.

In Antarctica, polar warming is limited mainly to the Antarctic Peninsula and West Antarctica (Amundsen-Bellingshausen seas)/ice shelves along the Peninsula are disintegrating. Sea ice, in contrast, has slightly expanded but there is large regional variation.

 

Read more on this topic:

from Professor David Walton in part 1 of the series

and from Professor Grant Bigg in part 3 of the series.

Enjoyed reading this article? Share it today:

About the Author: Roger Barry

Roger G. Barry was Director of the National Snow and Ice Data Center (NSIDC) at the University of Colorado Boulder from 1977 to 2008, and Professor of Geography from 1968 to 2010. He was appointed a University of Colorado Distinguished Professor in 2004. From 2012 to 2014 he was Director of the International CLIVAR Project Office, National Oceanogr...

View the Author profile >
 

Latest Comments

Have your say!